Related to Isotopic dating: radioactive dating , Radiometric dating , uniformitarianism. A method for determining the age of an object based on the concentration of a particular radioactive isotope contained within it and the half-life of that isotope. Also called: radioactive dating. A method for determining the age of an object based on the concentration of a particular radioactive isotope contained within it.
Isotope Analysis | Time Team America | PBS
The work of geologists is to tell the true story of Earth's history—more precisely, a story of Earth's history that is ever truer. A hundred years ago, we had little idea of the story's length—we had no good yardstick for time. Today, with the help of isotopic dating methods, we can determine the ages of rocks nearly as well as we map the rocks themselves. For that, we can thank radioactivity, discovered at the turn of the last century. A hundred years ago, our ideas about the ages of rocks and the age of the Earth were vague. But obviously, rocks are very old things.
Before the development of isotopic dating methods the age of the earth was estimated by quizlet
Originally fossils only provided us with relative ages because, although early paleontologists understood biological succession, they did not know the absolute ages of the different organisms. It was only in the early part of the 20th century, when isotopic dating methods were first applied, that it became possible to discover the absolute ages of the rocks containing fossils. In most cases, we cannot use isotopic techniques to directly date fossils or the sedimentary rocks they are found in, but we can constrain their ages by dating igneous rocks that cut across sedimentary rocks, or volcanic ash layers that lie within sedimentary layers.
Radiometric dating often called radioactive dating is a way to find out how old something is. The method compares the amount of a naturally occurring radioactive isotope and its decay products, in samples. The method uses known decay rates. It is the main way to learn the age of rocks and other geological features, including the age of the Earth itself.